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Inquiry Question 3: How does the force of gravity determine the motion of planets and satellites?

Apply qualitatively and quantitatively Newton's Law of Universal Gravitation, F = G m_1 m_2 / r^2, to determine the magnitude of force, gravitational field strength g = G M / r^2, and acceleration due to gravity at different points in a radial gravitational field

A focused answer to the HSC Physics Module 5 dot point on Newton's Law of Universal Gravitation. The inverse-square law, gravitational field strength, calculating g at different altitudes, and the worked surface-gravity example.

Reviewed by: AI editorial process; not yet individually human-reviewed

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  1. What this dot point is asking
  2. The answer
  3. Examples in context

What this dot point is asking

NESA wants you to apply Newton's Law of Universal Gravitation to calculate the force between two masses, determine the gravitational field strength at a point, and explain how the inverse-square dependence on distance shapes planetary and satellite motion. You need both the conceptual explanation (action at a distance, field model) and the numerical fluency to compute FF and gg at arbitrary distances.

The answer

Newton's Law of Universal Gravitation

Every pair of point masses attracts each other with a force directed along the line joining them:

F=Gm1m2r2F = G \frac{m_1 m_2}{r^2}

where:

  • G=6.67×1011 N m2kg2G = 6.67 \times 10^{-11}\ \text{N m}^2\,\text{kg}^{-2} is the universal gravitational constant.
  • m1m_1 and m2m_2 are the two masses in kilograms.
  • rr is the distance between their centres (not surfaces).

The force is mutual: each mass exerts the same magnitude of force on the other (Newton's third law).

The inverse-square law

Force is inversely proportional to the square of the distance. Doubling rr reduces the force to one quarter. Halving rr quadruples the force. This rapid fall-off explains why Earth's gravity dominates near the surface but becomes negligible far from the planet.

Inverse square law for gravitational force A plot of gravitational force F against distance r. The curve falls as one over r squared. At distance r the force is F. At distance 2 r the force is F over 4. At distance 3 r the force is F over 9. F r at r: F at 2r: F⁄4 at 3r: F⁄9 r 2r 3r F = G m₁m₂ ⁄ r². Doubling the separation quarters the force.

Gravitational field strength

The gravitational field strength gg at a point is the gravitational force per unit mass on a test mass placed there:

g=Fm=GMr2g = \frac{F}{m} = \frac{G M}{r^2}

where MM is the mass of the source body and rr is the distance from its centre. Units: N/kg or m/s2^2 (numerically equal).

At Earth's surface (r=RE=6.37×106r = R_E = 6.37 \times 10^6 m): g9.8 m/s2g \approx 9.8 \text{ m/s}^2.

The radial gravitational field

A gravitational field is a region of space in which a mass experiences a force. Around a spherical body the field is radial: the field vectors point toward the centre of the mass from every direction, and they get shorter (weaker) with distance, since g1/r2g \propto 1/r^2.

Radial gravitational field around a spherical mass A central sphere representing a planet with field vector arrows pointing radially inward toward its centre from eight directions around it. Arrows further from the sphere are shorter, showing that the field strength g decreases with distance according to the inverse square law. M shorter arrow far out: weaker field Field vectors point radially inward; length ∝ g ∝ 1 ⁄ r².

Acceleration due to gravity

For an object of mass mm in free fall in a gravitational field gg, the acceleration is a=ga = g (regardless of mm, because F=mgF = mg and a=F/ma = F/m). All objects fall with the same acceleration in a given gravitational field, in the absence of air resistance.

How gg decays with distance

Because g=GM/r2g = GM/r^2, plotting gg against rr for a fixed planet gives a curve that starts high at the surface and falls away steeply at first, then flattens as it approaches (but never reaches) zero at very large rr - the same 1/r21/r^2 shape as the force graph above, but for field strength rather than force.

Gravitational field strength g versus distance r for Earth A one over r squared decay curve of Earth's gravitational field strength g against distance r measured in Earth radii, starting near 9.8 metres per second squared at one Earth radius and falling steeply before flattening toward zero at larger distances. A data point at two Earth radii sits on the curve at a field strength of about 2.5 metres per second squared. distance r (Earth radii R_E) field strength g (m s⁻²) 12345 246810 at 2R_E: g ≈ 2.5 m s⁻² g = GM ⁄ r²: steep fall, then flattens toward zero.

Field model versus action at a distance

Two equivalent descriptions:

  • Action at a distance: the two masses pull on each other directly across empty space.
  • Field model: each mass creates a gravitational field around itself, and any other mass in that field experiences a force. The field model is preferred for HSC because it generalises cleanly to electric and magnetic fields.

Examples in context

Example 1. Gravitational pull on the Parkes 64 m dish. The Parkes radio telescope dish has a mass of 300,000 kg300{,}000 \text{ kg}. At Earth's surface (ME=5.97×1024 kgM_E = 5.97 \times 10^{24} \text{ kg}, rE=6.37×106 mr_E = 6.37 \times 10^6 \text{ m}), Newton's law gives F=GMEm/rE2=6.67×1011×5.97×1024×3.0×105/(6.37×106)2=2.94×106 NF = G M_E m / r_E^2 = 6.67 \times 10^{-11} \times 5.97 \times 10^{24} \times 3.0 \times 10^5 / (6.37 \times 10^6)^2 = 2.94 \times 10^6 \text{ N}. This is exactly mg=3×105×9.8=2.94×106 Nm g = 3 \times 10^5 \times 9.8 = 2.94 \times 10^6 \text{ N} as expected, confirming that the surface field strength g=GME/rE2=9.8 m/s2g = G M_E / r_E^2 = 9.8 \text{ m/s}^2 is the same for every mass.

Example 2. Moon-Earth attraction and ocean tides on the NSW coast. With Earth-Moon distance r=3.84×108 mr = 3.84 \times 10^8 \text{ m} and MMoon=7.35×1022 kgM_{\text{Moon}} = 7.35 \times 10^{22} \text{ kg}, the Moon's gravitational acceleration at Earth's centre is gM=GMMoon/r2=3.32×105 m/s2g_M = G M_{\text{Moon}} / r^2 = 3.32 \times 10^{-5} \text{ m/s}^2. The tidal effect along the Coffs Harbour tide gauge comes from the difference in gMg_M between Earth's near side and centre: Δg=2GMMoonrE/r3=1.10×106 m/s2\Delta g = 2 G M_{\text{Moon}} r_E / r^3 = 1.10 \times 10^{-6} \text{ m/s}^2. This 107g\sim 10^{-7} g differential pulls the ocean into the tidal bulges that NSW Ports records as roughly 1.5 m1.5 \text{ m} semidiurnal tides.

Exam-style practice questions

Practice questions written in the style of NESA exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.

2020 HSC4 marksCalculate the gravitational field strength at an altitude of 1000 km above the Earth's surface. (Mass of Earth = 5.97 x 10^24 kg, radius of Earth = 6.37 x 10^6 m, G = 6.67 x 10^-11 N m^2/kg^2.)
Show worked answer →

Gravitational field strength at distance rr from the centre of a mass MM:

g=GMr2g = \frac{G M}{r^2}.

The distance from the centre is r=RE+h=6.37×106+1.0×106=7.37×106r = R_E + h = 6.37 \times 10^6 + 1.0 \times 10^6 = 7.37 \times 10^6 m.

g=6.67×1011×5.97×1024(7.37×106)2g = \frac{6.67 \times 10^{-11} \times 5.97 \times 10^{24}}{(7.37 \times 10^6)^2}
g=3.98×10145.43×1013g = \frac{3.98 \times 10^{14}}{5.43 \times 10^{13}}
g=7.33 m/s2g = 7.33 \text{ m/s}^2.

Markers reward the correct use of r=RE+hr = R_E + h (not just hh), the substitution shown explicitly, and the final answer with units. A common student error is using altitude alone as rr.

2018 HSC3 marksExplain why the gravitational force on an astronaut in the International Space Station (altitude ~400 km) is only slightly less than at the Earth's surface, even though the astronaut experiences apparent weightlessness.
Show worked answer →

The gravitational force follows the inverse-square law F=GMmr2F = \frac{G M m}{r^2}. The astronaut is 400400 km above the surface, so the distance from Earth's centre changes from 63706370 km to 67706770 km. The ratio of forces is:

FISSFsurface=(63706770)20.89\frac{F_{\text{ISS}}}{F_{\text{surface}}} = \left(\frac{6370}{6770}\right)^2 \approx 0.89.

So gravity at the ISS is still about 89% of its surface value, around 8.7 m/s28.7 \text{ m/s}^2.

The astronaut feels weightless not because gravity is absent, but because both the astronaut and the station are in free fall around the Earth. They share the same gravitational acceleration, so there is no normal force between the astronaut and the floor, and no sensation of weight. Apparent weightlessness is a consequence of free fall, not the absence of gravity.

Markers reward the quantitative comparison, the distinction between gravitational force and apparent weight, and the link to free fall.

Practice questions

Original practice questions graded from foundation to exam level, each with a full worked solution. Try them before revealing the solution.

foundation2 marksState Newton's Law of Universal Gravitation in words and as an equation, defining every symbol and giving the value of GG.
Show worked solution →

Word statement. Every pair of point masses attracts each other with a force directed along the line joining them, proportional to the product of the masses and inversely proportional to the square of the distance between their centres.

Equation. F=Gm1m2r2F = \dfrac{Gm_1m_2}{r^2}, where FF is the gravitational force in newtons, m1m_1 and m2m_2 are the two masses in kilograms, rr is the distance between their centres in metres, and G=6.67×1011 N m2kg2G = 6.67 \times 10^{-11}\ \text{N m}^2\,\text{kg}^{-2} is the universal gravitational constant.

Marks: one for a correct word statement (inverse-square, proportional to both masses), one for the correct equation with every symbol defined and the value of GG given.

foundation3 marksCalculate the gravitational force between two 1000 kg1000\ \text{kg} spheres whose centres are 2.0 m2.0\ \text{m} apart. (G=6.67×1011 N m2kg2G = 6.67 \times 10^{-11}\ \text{N m}^2\,\text{kg}^{-2}.)
Show worked solution →

F=Gm1m2r2=(6.67×1011)(1000)(1000)(2.0)2F = \dfrac{Gm_1m_2}{r^2} = \dfrac{(6.67 \times 10^{-11})(1000)(1000)}{(2.0)^2}

F=6.67×1054.0=1.7×105 NF = \dfrac{6.67 \times 10^{-5}}{4.0} = 1.7 \times 10^{-5}\ \text{N}.

Marks: one for the correct formula with values substituted, one for correctly squaring rr, one for the answer stated to two significant figures with the unit newton.

foundation3 marksCalculate the gravitational field strength at the surface of the Moon. (MMoon=7.35×1022 kgM_{\text{Moon}} = 7.35 \times 10^{22}\ \text{kg}, RMoon=1.74×106 mR_{\text{Moon}} = 1.74 \times 10^6\ \text{m}.)
Show worked solution →

g=GMr2=(6.67×1011)(7.35×1022)(1.74×106)2g = \dfrac{GM}{r^2} = \dfrac{(6.67 \times 10^{-11})(7.35 \times 10^{22})}{(1.74 \times 10^6)^2}

g=4.90×10123.03×1012=1.6 m s2g = \dfrac{4.90 \times 10^{12}}{3.03 \times 10^{12}} = 1.6\ \text{m s}^{-2}.

Marks: one for the formula g=GM/r2g = GM/r^2, one for substituting the Moon's own mass and radius (not Earth's), one for the answer 1.6 m s21.6\ \text{m s}^{-2} with the unit. Note this is about one-sixth of Earth's surface value.

core4 marksA satellite of mass 500 kg500\ \text{kg} orbits at an altitude of 3000 km3000\ \text{km} above the Earth's surface. **(a)** Calculate the distance from the Earth's centre. **(b)** Calculate the gravitational force on the satellite at this altitude. (ME=5.97×1024 kgM_E = 5.97 \times 10^{24}\ \text{kg}, RE=6.37×106 mR_E = 6.37 \times 10^6\ \text{m}.)
Show worked solution →

(a) r=RE+h=6.37×106+3.0×106=9.37×106 mr = R_E + h = 6.37 \times 10^6 + 3.0 \times 10^6 = 9.37 \times 10^6\ \text{m}.

(b) F=GMEmr2=(6.67×1011)(5.97×1024)(500)(9.37×106)2F = \dfrac{GM_Em}{r^2} = \dfrac{(6.67 \times 10^{-11})(5.97 \times 10^{24})(500)}{(9.37 \times 10^6)^2}

F=1.99×10178.78×1013=2.3×103 NF = \dfrac{1.99 \times 10^{17}}{8.78 \times 10^{13}} = 2.3 \times 10^3\ \text{N}.

Marks: one for correctly finding r=RE+hr = R_E + h, one for the force formula with values substituted, one for correctly squaring rr, one for the answer 2.3×103 N2.3 \times 10^3\ \text{N} with the unit.

core4 marksThe figure shows how the gravitational field strength gg of the Earth varies with distance rr from its centre, with rr measured in Earth radii RER_E. **(a)** Describe the shape of the curve and the relationship it shows. **(b)** Use the data point on the graph to state the field strength at r=2REr = 2R_E. **(c)** Verify this reading using g=GM/r2g = GM/r^2. (ME=5.97×1024 kgM_E = 5.97 \times 10^{24}\ \text{kg}, RE=6.37×106 mR_E = 6.37 \times 10^6\ \text{m}.)
Show worked solution →

(a) The curve falls steeply at first and then flattens out, approaching (but never reaching) zero. This is the inverse-square relationship g=GM/r2g = GM/r^2: gg is proportional to 1/r21/r^2, so it decreases rapidly with distance but never becomes exactly zero.

(b) The marked data point at r=2REr = 2R_E reads g2.5 m s2g \approx 2.5\ \text{m s}^{-2}.

(c) r=2RE=2(6.37×106)=1.274×107 mr = 2R_E = 2(6.37 \times 10^6) = 1.274 \times 10^7\ \text{m}.

g=GMEr2=(6.67×1011)(5.97×1024)(1.274×107)2=3.98×10141.62×1014=2.5 m s2g = \dfrac{GM_E}{r^2} = \dfrac{(6.67 \times 10^{-11})(5.97 \times 10^{24})}{(1.274 \times 10^7)^2} = \dfrac{3.98 \times 10^{14}}{1.62 \times 10^{14}} = 2.5\ \text{m s}^{-2}.

Marks: one for describing the steep-then-flattening inverse-square shape, one for correctly reading g2.5 m s2g \approx 2.5\ \text{m s}^{-2} off the graph, one for the substitution r=2RE=1.274×107 mr = 2R_E = 1.274 \times 10^7\ \text{m}, one for the calculated value matching the graph reading.

core3 marksA person of mass 70 kg70\ \text{kg} stands on the Earth's surface. **(a)** Use Newton's Law of Universal Gravitation to calculate the gravitational force (weight) on them. **(b)** Show that this is consistent with W=mgW = mg using g=9.8 m s2g = 9.8\ \text{m s}^{-2}. (ME=5.97×1024 kgM_E = 5.97 \times 10^{24}\ \text{kg}, RE=6.37×106 mR_E = 6.37 \times 10^6\ \text{m}.)
Show worked solution →

(a) F=GMEmRE2=(6.67×1011)(5.97×1024)(70)(6.37×106)2=2.79×10164.06×1013=6.9×102 NF = \dfrac{GM_Em}{R_E^2} = \dfrac{(6.67 \times 10^{-11})(5.97 \times 10^{24})(70)}{(6.37 \times 10^6)^2} = \dfrac{2.79 \times 10^{16}}{4.06 \times 10^{13}} = 6.9 \times 10^2\ \text{N}.

(b) W=mg=70×9.8=6.9×102 NW = mg = 70 \times 9.8 = 6.9 \times 10^2\ \text{N}, matching part (a). This confirms that g=GME/RE2g = GM_E/R_E^2 is simply the constant of proportionality between an object's mass and its weight at the surface.

Marks: one for the correct force calculation with substitution, one for the answer 6.9×102 N6.9 \times 10^2\ \text{N} with the unit, one for showing mgmg gives the same value and stating the link between the two formulas.

exam6 marksAnalyse how Newton's Law of Universal Gravitation unified the explanation of an apple falling to the ground with the explanation of the Moon's orbit around the Earth.
Show worked solution →

Band-6 plan. (1) State the law and its inverse-square, universal character. (2) Apply it to the apple: near Earth's surface, rREr \approx R_E, giving g9.8 m s2g \approx 9.8\ \text{m s}^{-2}, a straight-line fall. (3) Apply it to the Moon: same law, much larger rr, giving a much smaller acceleration that curves the Moon's straight-line motion into an orbit rather than a fall to the surface. (4) State the unifying insight: the SAME force law, at different distances, explains both a fall and an orbit. Use numbers for both cases.

Model answer. Newton's Law of Universal Gravitation states that any two masses attract each other with a force F=Gm1m2/r2F = Gm_1m_2/r^2, directed along the line joining them and dependent only on the masses and the separation - the same law applies to every pair of masses in the universe, from an apple to a planet.

Near the Earth's surface an apple is at rRE=6.37×106 mr \approx R_E = 6.37 \times 10^6\ \text{m} from Earth's centre, giving a field strength g=GME/RE29.8 m s2g = GM_E/R_E^2 \approx 9.8\ \text{m s}^{-2}. The apple's initial horizontal velocity is zero, so this acceleration simply pulls it straight down to the ground - what everyone calls "falling".

The Moon experiences exactly the same law, but at r=3.84×108 mr = 3.84 \times 10^8\ \text{m}, roughly 60 times further from Earth's centre. Because the force falls as 1/r21/r^2, the Moon's gravitational acceleration toward Earth is about 602360060^2 \approx 3600 times smaller than at the surface, only around 2.7×103 m s22.7 \times 10^{-3}\ \text{m s}^{-2}. Unlike the apple, the Moon has a large tangential (sideways) velocity, so this weak acceleration does not pull it straight down - it continuously deflects the Moon's straight-line path into a closed curve, i.e. an orbit. In effect, the Moon is "falling" toward Earth forever but also moving sideways fast enough to keep missing it.

Newton's insight was that the apple and the Moon obey the identical inverse-square law of gravitation; the enormous difference in outcome (a fall versus a stable orbit) comes entirely from the difference in distance (which sets the size of gg) and tangential speed, not from any difference in the underlying force. This was the first demonstration that the same physical law governs motion on Earth and in the heavens.

Marker's note: the top band states the SAME equation applies to both scenarios, gives a numeric estimate of gg (or the force) for both the apple and the Moon, and explicitly explains why a weaker, more distant force produces an orbit rather than a fall (tangential velocity plus continuous deflection). A response that only asserts "the same law applies" without the distance/magnitude reasoning caps in the middle band.

exam6 marksEvaluate the claim that "gravity has a limited range and becomes zero once you are far enough from a planet", using Newton's Law of Universal Gravitation and the concept of a gravitational field.
Show worked solution →

Band-6 plan. (1) State the claim to be evaluated. (2) Use the inverse-square law to show force/field strength approaches zero asymptotically but never becomes exactly zero at any finite rr - so mathematically the claim is false. (3) Explain why the claim FEELS true in practice (the field becomes negligibly small very quickly because of the r2r^2 term, and other, closer masses dominate). (4) Reach a balanced judgement: technically false, but a reasonable practical approximation at large distances.

Model answer. The claim is that gravity has a definite cut-off distance beyond which it is exactly zero. Newton's Law of Universal Gravitation, F=Gm1m2/r2F = Gm_1m_2/r^2, shows this is not correct: for any finite separation rr, FF has some non-zero value, however small. As rr \to \infty, F0F \to 0, but this is an asymptotic limit - the force approaches zero without ever reaching it at a finite distance. The same is true of the field strength g=GM/r2g = GM/r^2: it decreases smoothly and continuously with rr, with no sudden drop to zero at any particular distance.

However, the claim captures a real physical effect: because the field falls as 1/r21/r^2, doubling the distance from a planet cuts the field to a quarter, and by ten times the distance the field is only one-hundredth as strong. Practically, the field becomes so small at large distances that it is completely swamped by the gravitational field of other, closer masses (for example, once far enough from Earth, the Sun's gravity dominates the motion of a spacecraft) or is simply too weak to have any measurable effect. This gives the everyday impression of a "boundary" to a planet's gravity, even though no true boundary exists.

On balance, the claim is technically false as a statement about the physics (gravity is unbounded in range and never reaches exactly zero), but it is a reasonable practical simplification: because of the rapid inverse-square fall-off, a planet's gravitational influence becomes negligible - though never mathematically zero - within a modest multiple of its own radius.

Marker's note: the top band explicitly distinguishes "approaches zero asymptotically" from "reaches zero at a finite distance", uses the 1/r21/r^2 dependence to justify why the field becomes negligible quickly in practice, and delivers an explicit judgement (technically false, practically reasonable) rather than a one-sided answer. A response that just says "gravity never ends" with no acknowledgement of the practical basis for the claim caps in the middle band.

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